作者: Hongmei Wang , Jerry M. Bigham , Olli H. Tuovinen
DOI: 10.1016/J.HYDROMET.2007.03.010
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摘要: Abstract This study evaluated the oxidation of research-grade marcasite and pyrite in shake flask experiments using iron-oxidizing bacteria archaea at 22, 45, 65 °C. Dissolved iron concentration pH were monitored intervals. The results showed that was more reactive than to both microbiological chemical oxidation. These are consistent with established structural thermodynamic differences between two minerals, which should make weathering